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Climate Change and Extreme Heat
September 25, 2023
The United States experienced a series of
record-breaking heat waves during the summer of 2023. The
heat waves brought extreme temperatures to various U.S. regions, including Puerto Rico, the southern
Plains, and the Northeast and Mid-Atlantic states, with life threatening conditions in some areas.
These heat waves are part of a trend of rising global temperatures. The National Aeronautics and Space
Administrati
on (NASA) and the National Oceanic and Atmospheric Administratio
n (NOAA) maintain
datasets of global average surface temperatures. According to these datasets, as of January 2023, the
warmest years since the advent of modern recordkeeping occurred in 2010-2022, with 2016 and 2020 tied
(i.e., statistically indistinguishable) as t
he warmest years on record (Figure 1).
Figure 1. Global Average Temperature Anomalies 1850-2022
Source: NOAA, National Centers for Environmental informatio
n, Climate at a Glance: Global Time Series.
Note: Global average temperature anomalies calculated as deviations from the 1901-2000 baseline average.
Independently developed global temperatures datasets that differ from the NASA and NOAA datasets in
duration and methodology, including analyses usin
g different baseline reference temperatures, show close
agreement (Figure 2) with respect to global temperatures and trends.
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Figure 2. Global Average Temperatures Anomalies: Four Independent Datasets
Source: Alan Buis, “The Raw Truth on Global Temperature Records,” National Aeronautics and Space Administration
(NASA), March 25, 2021
, https://climate.nasa.gov/explore/ask-nasa-climate/3071/the-raw-truth-on-global-temperature-
records/. Note: Global average temperature difference from a baseline reference average value (1951-1980).
The Connection Between Human-Influenced Climate Change and
Extreme Heat
The observed rising global temperatures are associated with increasingly frequent and intense climate
change impacts, including extreme high temperatures and periods of abnormally hot weather known as
heat waves. The Intergovernmental Panel on Climate Change (IPCC)
Sixth Assessment Report states (with
associated confidence levels) the following:
The frequency and intensity of hot extremes (including heatwaves) have increased, and those of
cold extremes have decreased on the global scale since 1950 (virtually certain).
Climate change attribution is the study of whether, or to what degree, human influence may have
contributed to extreme climate or weather events. Some climate change attribution studies of
extreme heat
events in the United States from 2011 to 2014 have attributed increases in the frequency or intensity of
thes
e extreme heat events to human-influenced climate change. Human-driven emissions of greenhouse
gases are likely to be the cause of the increased temperatures that have been associated with these extreme
heat events. The U.S. Global Change Research Program (USGCR
P) Fourth National Climate Assessment
(NCA4) states, “It is extremely likely that human activities, especially emissions of greenhouse gases, are
the dominant cause of the observed warming since the mid-20th century.” Similarly, the IPCC Sixth
Assessment Report states that “human-induced greenhouse gas forcing is the main driver of the observed
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changes in hot and cold extremes on the global scale (virtually certain) and on most continents (very
likely).”
Climate Change and Estimates of Future Extreme Heat
The NCA4, using scenarios of greenhouse gas emissions and climate policies, states that “statistically
significant warming is projected for all parts of the United States throughout the century.” This warming
is part of the ongoing, observed
global increase in average temperature discussed above. Researchers
measure this increase by comparing the current and projected global average temperatures with a
historical period before large-scale industrialization, such as 1850-1900 (pre-industrial period). The
estimat
ed warming level in June 2023 was 1.2oC (2.2oF), indicating that the global temperature has risen
1.2oC (2.2oF) since the pre-industrial period.
The Paris Agreement climate treaty recognizes that limiting
warming to 1.5oC (2.7oF) reduces climate change risk and impacts. The IPCC estimates warming may
reach the 1.5oC (2.7oF) level between
2030 and 2052.
Increases in global average temperature affect the way the climate behaves
, including the incidence of
heat extremes. While there i
s no universally agreed on definition of extreme heat,
one IPCC metric is the
average annual number of days in which temperatures exceed thresholds of 35oC (95oF) and 40oC
(104oF), compared with a 1986-2005 baseline period. These temperature thresholds have been associated
with adverse impacts o
n agriculture and human health.
In model
s presented by the IPCC, the average annual number of extreme heat days for geographic regions
containing the United States would increase under global warming potentially occurring during the 21st
century. Estimates of extreme heat associated with global warming may change with scientific
developments.
Considerations for Congress
The 117th Congress passed the legislation known as the
Inflation Reduction Act and t
he Infrastructure
Investment and Jobs Act, which, among other goals, aimed to address extreme heat by reducing climate-
changing greenhouse gas emissions. Example activities included
• enhancing electricity grid resilience,
• reducing the impacts on transportation infrastructure, and
• reducing urban heat islands.
Members of the 118th Congress have expressed interest in addressing the health effects of extreme heat
and improving the preparation and response to heat waves and other extreme heat events.
The Biden Administration has announc
ed activities to address extreme heat, which are subject to
congressional oversight. They include the formation of t
he National Integrated Heat Health Information
System, a collaborative effort by the Centers for Disease Control and Prevention (CDC), NOAA, and
other federal agencies, as well as activities funded under the Inflation Reduction Act that include grants to
increase urban green spaces, loans to upgrade residences to provide protection from extreme heat, and
improvements t
o extreme heat forecasting by NOAA.
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Author Information
Jonathan D. Haskett
Analyst in Environmental Policy
Disclaimer
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